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SU0012885 SSNL
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SU0012885 SSNL
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Last modified
1/14/2020 4:18:23 PM
Creation date
9/4/2019 10:53:26 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0012885
PE
2611
FACILITY_NAME
SU-92-15
STREET_NUMBER
8721
Direction
N
STREET_NAME
CANEPA
STREET_TYPE
RD
City
STOCKTON
Zip
95212-
APN
08640008
ENTERED_DATE
1/14/2020 12:00:00 AM
SITE_LOCATION
8721 N CANEPA RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\sballwahn
Supplemental fields
FilePath
\MIGRATIONS\C\CANEPA\8721\SU-92-15_SU-87-21\NL STDY.PDF
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EHD - Public
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•; # kn KLEINFELDER <br /> File No. 20-2921-01 <br /> March 25, 1992 <br /> hours. The last 30 minutes of each test were used to <br /> calculate the percolation rates. In order to use standard <br /> leach lines, the County requires a percolation rate of 60 <br /> minutes per inch, or faster, at the 3-foot depth. In order <br /> to use sump pits, the County requires a soil strata with a <br /> percolation rate of 30 minutes per inch, or faster, be <br /> located. <br /> Based on the above criteria, two approximate 3-foot deep, <br /> three approximate 8-foot deep and one approximate 14-foot <br /> deep tests produced passing percolation rates. The following <br /> table presents the percolation rates and depths for each lot <br /> tested. The County approved percolation test sheets are <br /> included with this report. <br /> PERCOLATION TEST RESULTS <br /> Depth Percolation Rate <br /> Test/Lot No. feet (mins/inch) _ <br /> P-1/Lot 1 8-1/2 15 <br /> P-2/Lot 17 8 12 <br /> P-3/Lot 25 8-1/2 6 <br /> P-4/Lot 11 3-1/2 8-1/2 <br /> P-5/Lot 36 3 24 <br /> P-6/Lot 18 14 6 <br /> We note that prior to final approval for construction, the County <br /> will require a passing percolation test be obtained at each lot. <br /> We will be happy to prepare a proposal for performing the <br /> additional percolation testing. <br /> ITEM C-3: <br /> t "The depth and gradient of the water table;" <br /> s <br /> During our residence surveys between February 27 and March 9, <br /> 1992, we .were not able to measure groundwater in the domestic <br /> wells. The regional groundwater depth map published by the <br /> San Joaquin County Flood Control and Water Conservation <br /> District, Plate II, indicates the depth to groundwater in the <br /> site area was approximately 90 to 95 feet in spring 1991. <br /> Based on the groundwater map showing lines of equal elevation <br /> of groundwater, Plate III, we conclude that the main <br /> g gradient radient is in roughly the south-southeast <br /> direction. <br /> Copyright 1992 Kleinfelder, Inc. Page 3 of 9 <br />
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